The Bannock Burn (Scottish Gaelic: Allt a' Bhonnaich) is a stream (burn is Scots for stream) which rises in the Touch Hills to the south-west of Stirling in central Scotland. The Bannock flows eastward and enters the River Forth to the east of Stirling, close to the site of the Battle of Bannockburn (1314). A nearby town, nowadays a suburb of Stirling, is accordingly called Bannockburn.
The Battle of Sauchieburn (1488) was also fought close to the Bannock Burn.
The upper part of the valley of the Bannock Burn appears to have been inhabited in the Iron Age. Several duns are to be found in the Graigend and Murrayshall area and a fort on Lewis Hill. The Dun at Murrayshall (NS774908) was partly excavated in 1967. A few minor artifacts were found. Other duns in the area are Walstale, Castlehill 1, Castlehill 2, and Castlehill Wood. Another ruined fort is located on the NW side of Gillies Hill.
In the upper part of the Bannock valley there is a reservoir at North Third, which supplies water to the petrochemical complex at Grangemouth.
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—Samuel Daniel (15621619)